Danish pollen records radiocarbon‐dated to between 50000 and 57000 yr BP
Identifieur interne : 001481 ( Istex/Corpus ); précédent : 001480; suivant : 001482Danish pollen records radiocarbon‐dated to between 50000 and 57000 yr BP
Auteurs : Else KolstrupSource :
- Journal of Quaternary Science [ 0267-8179 ] ; 1992-06.
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Abstract
Radiocarbon‐dated pollen diagrams from four Danish sequences are presented in their sedimentological context. The pollen diagrams indicate the former presence of stands of Betula and Pinus and of Ericales, Poaceae, Cyperaceae and other herbs. From a straightforward comparison with other diagrams, one of the present series is tentatively correlated with part of the Early Weichselian Brørup Interstadial and two with parts of the Odderade Interstadial, which has not been demonstrated previously in Denmark. One diagram and part of another do not seem to match previously published records in northwest Europe. Yet, the possibility that the sediments date to hitherto unrecorded periods with environmental conditions similar to those reflected in known Weichselian deposits is not excluded. In two of the sequences high percentages of charcoal particles suggest the former occurrence of fires, which influenced the palaeovegetation and soil surface stability. It is suggested that counting of charcoal particles is included in future investigations in order to establish whether periods with fires can be identified in the sedimentary sequences.
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DOI: 10.1002/jqs.3390070207
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ISTEX:234382E56B4F173219C980E44AC8F794CEFE8D90Le document en format XML
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The pollen diagrams indicate the former presence of stands of Betula and Pinus and of Ericales, Poaceae, Cyperaceae and other herbs. From a straightforward comparison with other diagrams, one of the present series is tentatively correlated with part of the Early Weichselian Brørup Interstadial and two with parts of the Odderade Interstadial, which has not been demonstrated previously in Denmark. One diagram and part of another do not seem to match previously published records in northwest Europe. Yet, the possibility that the sediments date to hitherto unrecorded periods with environmental conditions similar to those reflected in known Weichselian deposits is not excluded. In two of the sequences high percentages of charcoal particles suggest the former occurrence of fires, which influenced the palaeovegetation and soil surface stability. It is suggested that counting of charcoal particles is included in future investigations in order to establish whether periods with fires can be identified in the sedimentary sequences.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>Else Kolstrup</name><affiliations><json:string>Mosevej 12, Blans, DK ‐ 6400 Sønderborg, Denmark</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>Denmark</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Weichselian</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>pollen analysis</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>radiocarbon dating</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>natural fires</value></json:item></subject><articleId><json:string>JQS3390070207</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>Radiocarbon‐dated pollen diagrams from four Danish sequences are presented in their sedimentological context. The pollen diagrams indicate the former presence of stands of Betula and Pinus and of Ericales, Poaceae, Cyperaceae and other herbs. From a straightforward comparison with other diagrams, one of the present series is tentatively correlated with part of the Early Weichselian Brørup Interstadial and two with parts of the Odderade Interstadial, which has not been demonstrated previously in Denmark. One diagram and part of another do not seem to match previously published records in northwest Europe. Yet, the possibility that the sediments date to hitherto unrecorded periods with environmental conditions similar to those reflected in known Weichselian deposits is not excluded. In two of the sequences high percentages of charcoal particles suggest the former occurrence of fires, which influenced the palaeovegetation and soil surface stability. It is suggested that counting of charcoal particles is included in future investigations in order to establish whether periods with fires can be identified in the sedimentary sequences.</abstract><qualityIndicators><score>7.004</score><pdfVersion>1.3</pdfVersion><pdfPageSize>612 x 828 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>1146</abstractCharCount><pdfWordCount>5730</pdfWordCount><pdfCharCount>35218</pdfCharCount><pdfPageCount>10</pdfPageCount><abstractWordCount>167</abstractWordCount></qualityIndicators><title>Danish pollen records radiocarbon‐dated to between 50000 and 57000 yr BP</title><refBibs><json:item><author><json:item><name>L. Aario</name></json:item></author><host><volume>LIV</volume><pages><first>120</first></pages><issue>8</issue><author></author><title>Annales Academiae Scientiarium Fennicae A</title></host><title>Waldgrenzen und subrezenten Pollenspektren in Petsamo Lappland</title></json:item><json:item><author><json:item><name>S. T. 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Part II: Middle Weichselian</title></json:item></refBibs><genre><json:string>article</json:string></genre><host><volume>7</volume><publisherId><json:string>JQS</json:string></publisherId><pages><total>10</total><last>172</last><first>163</first></pages><issn><json:string>0267-8179</json:string></issn><issue>2</issue><subject><json:item><value>Article</value></json:item></subject><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1099-1417</json:string></eissn><title>Journal of Quaternary Science</title><doi><json:string>10.1002/(ISSN)1099-1417</json:string></doi></host><categories><wos><json:string>science</json:string><json:string>geosciences, multidisciplinary</json:string><json:string>geography, physical</json:string></wos><scienceMetrix><json:string>natural sciences</json:string><json:string>earth & environmental sciences</json:string><json:string>paleontology</json:string></scienceMetrix></categories><publicationDate>1992</publicationDate><copyrightDate>1992</copyrightDate><doi><json:string>10.1002/jqs.3390070207</json:string></doi><id>234382E56B4F173219C980E44AC8F794CEFE8D90</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/234382E56B4F173219C980E44AC8F794CEFE8D90/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/234382E56B4F173219C980E44AC8F794CEFE8D90/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/234382E56B4F173219C980E44AC8F794CEFE8D90/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Danish pollen records radiocarbon‐dated to between 50000 and 57000 yr BP</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>John Wiley & Sons, Ltd</publisher><pubPlace>Essex</pubPlace><availability><p>Copyright © 1992 John Wiley & Sons, Ltd</p></availability><date>1992</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Danish pollen records radiocarbon‐dated to between 50000 and 57000 yr BP</title><author xml:id="author-1"><persName><forename type="first">Else</forename><surname>Kolstrup</surname></persName><affiliation>Mosevej 12, Blans, DK ‐ 6400 Sønderborg, Denmark</affiliation></author></analytic><monogr><title level="j">Journal of Quaternary Science</title><title level="j" type="abbrev">J. 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It is suggested that counting of charcoal particles is included in future investigations in order to establish whether periods with fires can be identified in the sedimentary sequences.</p></abstract><textClass xml:lang="en"><keywords scheme="keyword"><list><head>keywords</head><item><term>Denmark</term></item><item><term>Weichselian</term></item><item><term>pollen analysis</term></item><item><term>radiocarbon dating</term></item><item><term>natural fires</term></item></list></keywords></textClass><textClass><keywords scheme="Journal Subject"><list><head>article-category</head><item><term>Article</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1991-11-15">Received</change><change when="1992-03-04">Registration</change><change when="1992-06">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/234382E56B4F173219C980E44AC8F794CEFE8D90/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component version="2.0" type="serialArticle" xml:lang="en"><header><publicationMeta level="product"><publisherInfo><publisherName>John Wiley & Sons, Ltd</publisherName><publisherLoc>Essex</publisherLoc></publisherInfo><doi registered="yes">10.1002/(ISSN)1099-1417</doi><issn type="print">0267-8179</issn><issn type="electronic">1099-1417</issn><idGroup><id type="product" value="JQS"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="JOURNAL OF QUATERNARY SCIENCE">Journal of Quaternary Science</title><title type="short">J. Quaternary Sci.</title></titleGroup></publicationMeta><publicationMeta level="part" position="20"><doi origin="wiley" registered="yes">10.1002/jqs.v7:2</doi><numberingGroup><numbering type="journalVolume" number="7">7</numbering><numbering type="journalIssue">2</numbering></numberingGroup><coverDate startDate="1992-06">June 1992</coverDate></publicationMeta><publicationMeta level="unit" type="article" position="7" status="forIssue"><doi origin="wiley" registered="yes">10.1002/jqs.3390070207</doi><idGroup><id type="unit" value="JQS3390070207"></id></idGroup><countGroup><count type="pageTotal" number="10"></count></countGroup><titleGroup><title type="articleCategory">Article</title><title type="tocHeading1">Articles</title></titleGroup><copyright ownership="publisher">Copyright © 1992 John Wiley & Sons, Ltd</copyright><eventGroup><event type="manuscriptReceived" date="1991-11-15"></event><event type="manuscriptAccepted" date="1992-03-04"></event><event type="firstOnline" date="2006-07-26"></event><event type="publishedOnlineFinalForm" date="2006-07-26"></event><event type="xmlConverted" agent="Converter:JWSART34_TO_WML3G version:2.3.2 mode:FullText source:HeaderRef result:HeaderRef" date="2010-03-15"></event><event type="xmlConverted" agent="Converter:WILEY_ML3G_TO_WILEY_ML3GV2 version:3.8.8" date="2014-02-01"></event><event type="xmlConverted" agent="Converter:WML3G_To_WML3G version:4.1.7 mode:FullText,remove_FC" date="2014-10-30"></event></eventGroup><numberingGroup><numbering type="pageFirst">163</numbering><numbering type="pageLast">172</numbering></numberingGroup><linkGroup><link type="toTypesetVersion" href="file:JQS.JQS3390070207.pdf"></link></linkGroup></publicationMeta><contentMeta><countGroup><count type="figureTotal" number="9"></count><count type="tableTotal" number="1"></count><count type="referenceTotal" number="25"></count></countGroup><titleGroup><title type="main" xml:lang="en">Danish pollen records radiocarbon‐dated to between 50000 and 57000 yr BP</title><title type="short" xml:lang="en">DANISH POLLEN RECORDS DATED TO BETWEEN 50000 AND 57000 YR BP</title></titleGroup><creators><creator xml:id="au1" creatorRole="author" affiliationRef="#af1"><personName><givenNames>Else</givenNames><familyName>Kolstrup</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="af1" countryCode="DK" type="organization"><unparsedAffiliation>Mosevej 12, Blans, DK ‐ 6400 Sønderborg, Denmark</unparsedAffiliation></affiliation></affiliationGroup><keywordGroup xml:lang="en" type="author"><keyword xml:id="kwd1">Denmark</keyword><keyword xml:id="kwd2">Weichselian</keyword><keyword xml:id="kwd3">pollen analysis</keyword><keyword xml:id="kwd4">radiocarbon dating</keyword><keyword xml:id="kwd5">natural fires</keyword></keywordGroup><abstractGroup><abstract type="main" xml:lang="en"><title type="main">Abstract</title><p>Radiocarbon‐dated pollen diagrams from four Danish sequences are presented in their sedimentological context. The pollen diagrams indicate the former presence of stands of <i>Betula</i> and <i>Pinus</i> and of Ericales, Poaceae, Cyperaceae and other herbs. From a straightforward comparison with other diagrams, one of the present series is tentatively correlated with part of the Early Weichselian Brørup Interstadial and two with parts of the Odderade Interstadial, which has not been demonstrated previously in Denmark. One diagram and part of another do not seem to match previously published records in northwest Europe. Yet, the possibility that the sediments date to hitherto unrecorded periods with environmental conditions similar to those reflected in known Weichselian deposits is not excluded. In two of the sequences high percentages of charcoal particles suggest the former occurrence of fires, which influenced the palaeovegetation and soil surface stability. It is suggested that counting of charcoal particles is included in future investigations in order to establish whether periods with fires can be identified in the sedimentary sequences.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Danish pollen records radiocarbon‐dated to between 50000 and 57000 yr BP</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>DANISH POLLEN RECORDS DATED TO BETWEEN 50000 AND 57000 YR BP</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Danish pollen records radiocarbon‐dated to between 50000 and 57000 yr BP</title></titleInfo><name type="personal"><namePart type="given">Else</namePart><namePart type="family">Kolstrup</namePart><affiliation>Mosevej 12, Blans, DK ‐ 6400 Sønderborg, Denmark</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>John Wiley & Sons, Ltd</publisher><place><placeTerm type="text">Essex</placeTerm></place><dateIssued encoding="w3cdtf">1992-06</dateIssued><dateCaptured encoding="w3cdtf">1991-11-15</dateCaptured><dateValid encoding="w3cdtf">1992-03-04</dateValid><copyrightDate encoding="w3cdtf">1992</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="figures">9</extent><extent unit="tables">1</extent><extent unit="references">25</extent></physicalDescription><abstract lang="en">Radiocarbon‐dated pollen diagrams from four Danish sequences are presented in their sedimentological context. The pollen diagrams indicate the former presence of stands of Betula and Pinus and of Ericales, Poaceae, Cyperaceae and other herbs. From a straightforward comparison with other diagrams, one of the present series is tentatively correlated with part of the Early Weichselian Brørup Interstadial and two with parts of the Odderade Interstadial, which has not been demonstrated previously in Denmark. One diagram and part of another do not seem to match previously published records in northwest Europe. Yet, the possibility that the sediments date to hitherto unrecorded periods with environmental conditions similar to those reflected in known Weichselian deposits is not excluded. In two of the sequences high percentages of charcoal particles suggest the former occurrence of fires, which influenced the palaeovegetation and soil surface stability. It is suggested that counting of charcoal particles is included in future investigations in order to establish whether periods with fires can be identified in the sedimentary sequences.</abstract><subject lang="en"><genre>keywords</genre><topic>Denmark</topic><topic>Weichselian</topic><topic>pollen analysis</topic><topic>radiocarbon dating</topic><topic>natural fires</topic></subject><relatedItem type="host"><titleInfo><title>Journal of Quaternary Science</title></titleInfo><titleInfo type="abbreviated"><title>J. Quaternary Sci.</title></titleInfo><genre type="journal">journal</genre><subject><genre>article-category</genre><topic>Article</topic></subject><identifier type="ISSN">0267-8179</identifier><identifier type="eISSN">1099-1417</identifier><identifier type="DOI">10.1002/(ISSN)1099-1417</identifier><identifier type="PublisherID">JQS</identifier><part><date>1992</date><detail type="volume"><caption>vol.</caption><number>7</number></detail><detail type="issue"><caption>no.</caption><number>2</number></detail><extent unit="pages"><start>163</start><end>172</end><total>10</total></extent></part></relatedItem><identifier type="istex">234382E56B4F173219C980E44AC8F794CEFE8D90</identifier><identifier type="DOI">10.1002/jqs.3390070207</identifier><identifier type="ArticleID">JQS3390070207</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright © 1992 John Wiley & Sons, Ltd</accessCondition><recordInfo><recordContentSource>WILEY</recordContentSource><recordOrigin>John Wiley & Sons, Ltd</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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